Abstract
The Garonne River drains an important part of the northern Pyrenees and its northern foreland. We investigated the middle reaches of the Garonne River establishing a detailed morphogenetic profile of its foreland terrace staircase and the preserved palaeoglacier margins. We particularly focussed on the glaciofluvial interface, linking (also genetically) the fluvial sediment archives in the foreland with the terminal glacial basin upstream of the Pyrenees mountain front. Using cosmogenic nuclide
Original language | English |
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Pages (from-to) | 71-95 |
Journal | Geomorphology |
Volume | 207 |
DOIs | |
Publication status | Published - 2014 |